Show ill I 1 1 lit I 1 I 1 I 1 T nr apal 21 dpn radin oil Drill drilling ind I 1 A ff W wf AAA al 11 n Z j drilling will bein bezin sometime this morth worth on the list chance structure which is located in the tile southwestern corner of emery the southeastern corner of sevier seier and the northan north rn pirt of 0 VV stayne countes coun res utah which includes larts of townships 2 and 27 rang ranges 5 6 and 7 eist and include includes 30 acres sll all goern government ment land which is covered by 19 oil and gi i permit these permits are held by local keople ind nd were turned to arthur E babson and earl 0 anderson ot price under tinder drilling and operating agreements who have inte restel john TV weightman claude E bowers E V falgren and bussel russel hi all of los 1 ft ill test the structure tute to the bottom of the Penns laurin formation un pm commercial production is in tn countered before re athing tin this depth it is estimated that the bottom of the can call be reached in feet the well will start i i the carmel limestone upper jurassic pene trat ing the navajo Isa vojo and win pate gate 0 of f the lower jurassic the Chin lee ani and moenkopi Moen kopi of the tri aniie the kaibab limestone linest oae and the coconino sandstone of the bermain series and the goo droge or of the carbon the latter formation is prod of gravity oil wherever he rever fenet penetrated rated by the drill in eastern altah where the test is I 1 properly erly made ninde on the structure these tests will 11 ll ib 1 I lucae the salt valley well the cirank well the boundary nutte butte well the shallow well in the in tuan titan oil field of rutih and abo tb deep test on the Hattle nake true ture jett 01 oer er the line in nor thet ern new ew mexico other strata which will be pene grated by the last chance test iho how oil seepages and asphalt ledges in dozens of places both north and 4 south of the structure the lut lirt chance chalice is an asymmetry fil ell f il anticline li hiving aing dir of from if to 10 0 degrees on the north and e rt M and from 3 to 5 decrees degrees on the s ith and west it rt has a closure of ir proximately feet this anti dine is mentioned in IT 8 S geology nl ril bulletin no 0 by geologist times W gullady who made wide a very f ireful and complete survey and report on all of the ge geological ologie al form potions underlying and inc include ludel I 1 in lit the tile western flank of the great ban fafael uplift this work wa done by mr nir guiltily and mr ur in 1 24 and sud MS but was not reported until 1429 in view of the fact that arbou dioxide gas was wai found at the farn hani ham and woodside structures on tl if e northern flank of the san rafael up lift and also in view of the fact that this gals ya is tsei efarin ef apin ping agh a fault plane south of chelp ant lelta i and north of the last chance an tiline it ii 11 expected that large of it mil will be found in tit ile coconino raid maidstone Mi stone at a depth of approximate iv 2774 feet A stan stallard lard tig rig will to I 1 c cited and the hole started wil be inches in diameter lalit IV W s t noted 0 1 operator ore rater from front loi toi angelee aill ill be in a of epe operations rations supplies will be hauled HI in from price ana and tre tte nearby tawni of all tho the well hue haie been beef drilled drill eil in lantern utah hare have had the surf ice show showing Ingi found in the icinia ici nit of the lat lait chance the structural condi ae ve a e ideal an I 1 at least four ga C cil 11 fonn form ution which e the same me at hala ow dittli show stor ol 01 seepages see pages or vf oil where the eime is exposed exposed b L erosion or has been pen by the dri lal work will be lushel ushel as a rapidly as is consistent with good manage meat |